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Habitat-Forming Seaweeds in a Changing Climate


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Titel: Habitat-Forming Seaweeds in a Changing Climate
Författare: Kinnby, Alexandra
E-post: alexandra.kinnby@marine.gu.se
Utgivningsdatum: 19-maj-2021
Universitet: Göteborgs universitet. Naturvetenskapliga fakulteten
Institution: Department of Marine Sciences ; Institutionen för marina vetenskaper
Delarbeten: PAPER I: Kinnby, A., Jonsson, P. R., Ortega-Martinez, O., Töpel, M., Pavia, H., Pereyra, R. T., & Johannesson, K. (2020). Combining an Ecological Experiment and a Genome Scan Show Idiosyncratic Responses to Salinity Stress in Local Populations of a Seaweed. Frontiers in Marine Science, 7, 470.
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PAPER II: Kinnby, A., White, J.C.B., Toth, G.B., & Pavia, H. (2021). Ocean acidification decreases grazing pressure but alters morphological structure in a dominant coastal seaweed. PloS one, 16(1), e0245017.
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PAPER III: Kinnby, A., Cervin, G., Larsson, A.I., Edlund, U., Toth, G.B., & Pavia, H. Increased risk of tissue breakage in habitat-forming seaweeds under ocean acidification. (Manuscript).

PAPER IV: Kinnby A. Toth G.B. & Pavia H. Climate change increases susceptibility to grazers in a foundation seaweed. (In review).

PAPER V: Kinnby, A., Johannesson, K., Cervin, G., & Pavia, H. Effects of ocean acidification and warming on fertilization success and germination in Fucus vesiculosus. (Manuscript).
Datum för disputation: 2021-06-09
Disputation: Onsdagen den 9 juni, 2021. kl. 08.00 i hörsalen på Tjärnö marina laboratorium, institutionen för marina vetenskaper, Laboratorievägen 10, 452 96 Strömstad.
Examinationsnivå: Doctor of Philosophy
Publikationstyp: Doctoral thesis
Nyckelord: Ocean acidification
Warming
Freshening
Temperature
Salinity
pH
pCO2
Fucus vesiculosus
Phlorotannins
Grazing
Tissue resilience
Macroalgae
Sammanfattning: Climate change is an umbrella term encompassing some of the largest and most potent selective pressures currently acting on ecosystems. It can have diverse effects on marine systems; the most powerful of which are changes to salinity through altered patterns of precipitation and evaporation, temperature through increased global temperature, and pH through the dissolution of CO2 into seawater where it ultimately reacts with water to form carbonate (CO32-) and hydrogen ions (2H+). All these change... mer
ISBN: 978-91-8009-360-6
URI: http://hdl.handle.net/2077/68048
Samling:Doctoral Theses from University of Gothenburg / Doktorsavhandlingar från Göteborgs universitet
Doctoral Theses / Doktorsavhandlingar Institutionen för marina vetenskaper

 

 

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